Mineralogical comparison of Antarctic and non-Antarctic HED (howardites-eucrites-diogenites) achondrites
スポンサーリンク
概要
- 論文の詳細を見る
Mineralogical examination of thin sections of non-Antarctic and Antarctic HED (howardite, eucrite, diogenite) achondrites indicates that they contain a variety of lithic components. Some of these components occur both as monomict meteorites and as clasts in polymict meteorites, whereas others occur only as clasts in some polymict breccias. The components may be classified by the degree of homogenization of the pyroxene present. In order of increasing homogeneity these are : (1) Y-75011-type basalt clasts; (2) Pasamonte; (3) Y-790266-type clasts; (4) Stannern and Nuevo Laredo; (5) Juvinas and Haraiya; and (6) Ibitira (?). Type 1 has been least modified by post-igneous thermal annealing, while types 5 and 6 were thoroughly metamorphosed. Three types of cumulate eucrites are recognized and are believed to represent (a) cumulates from thick lava flows or layered intrusions; (b) lunar highlands type crust; and (c) differentiation products of diogenitic magmas.
- 国立極地研究所の論文
著者
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TAKEDA Hiroshi
Research Institute, Chiba Institute of Technology
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Prinz M.
Department Of Earth And Planetary Sciences American Museum Of Natural History
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Prinz M.
Department Of Mineral Sciences Americal Museum Of Natural History
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Ishii Teruaki
Ocean Research Institute, University of Tokyo
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Takeda Hiroshi
Mineralogical Institute, University of Tokyo
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Takeda Hiroshi
Department Of Earth And Planetary Science The University Of Tokyo
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Mori Hiroshi
Mineralogical Institute, Faculty of Science, University of Tokyo
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Delaney J.S.
Department of Mineral Sciences, Americal Museum of Natural History
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Harlow G.E.
Department of Mineral Sciences, Americal Museum of Natural History
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Ishii Teruaki
Ocean Research Institute The University Of Tokyo
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Harlow G.e.
Department Of Mineral Sciences Americal Museum Of Natural History
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Delaney J.s.
Department Of Mineral Sciences Americal Museum Of Natural History
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Takeda Hiroshi
Mineralogical Institute Faculty Of Science University Of Tokyo
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Mori Hiroshi
Mineralogical Institute Faculty Of Science University Of Tokyo
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